Добавил:
Опубликованный материал нарушает ваши авторские права? Сообщите нам.
Вуз: Предмет: Файл:
Майнор / Книги / Chapter-5---Forced-convection_2021_Heat-Transfer-Engineering.pdf
Скачиваний:
0
Добавлен:
08.05.2026
Размер:
2.69 Mб
Скачать

 

 

 

 

 

 

5.5 Turbulent flow 147

and

 

 

qtotal = ρcp (α +εH )

 

 

 

T

(5.159)

 

y

 

 

The challenge though is to get the two quantities εm and εH . We now have three equations and five unknowns, namely, u, v, T , εm , and εH . This is the fundamental problem of closure in turbulence modeling. We need to relate εm and εH to the average quantities u, v , or T so that we can effectively handle the problem of closure. This activity is actually a separate field by itself and is known as turbulence modeling.

A quick look at the qualitative nature of the velocity profiles in laminar and turbulent boundary layers is in order. The turbulent velocity profile is sharp, with a steep slope at y = 0, denoting higher shear stress at the wall (see Fig. 5.7). Discerning readers will quickly realise that the higher shear stress at the wall will lead to more heat transfer. While the former is not desirable, the latter is.

The ratio of εm to εH is known as turbulent Prandtl number denoted by PrT . Similar to being nearly equal to in gases, εm /εH is nearly equal to 1.

 

εm

= PrT

≈ 1(for gases)

(5.160)

εH

 

 

 

 

For Pr >>1 fluids, based on boundary layer measurements, the recommended value of PrT is around 0.9. The idea of a turbulent Prandtl number, which is strictly not a physical property and is apparently intangible, is a useful construct in heat transfer engineering, as from five unknowns, we have eliminated one.

Reynolds analogy

Let us now see if we establish a relationship between momentum transfer and heat transfer. If we are successful in doing this, then by performing the easier-to-do velocity measurements together with the use of Newton’s law of viscosity, we can

FIGURE 5.7

Figure showing a qualitative variation of horizontal velocity in (A) laminar and (B) turbulent boundary layers over a flat plate.

148CHAPTER 5  Forced convection

obtain τ w, and from this we can get q. This will indeed be a godsend, and inductively we can extend the logic or more precisely the “analogy” to mass transfer itself. The idea of obtaining heat transfer results from cold flow measurements is plain brilliant!

Let us use the results of the integral solution to see if we can establish the analogy quantitatively.

Q

=

hA

(Tw T)

τ w

cf

×

1

2

 

 

2

ρu

 

 

 

 

 

 

 

 

T

 

Q = -k

 

 

 

 

 

 

y y=0

 

 

 

u

 

τ w = µ

 

 

 

 

 

 

y y=0

(5.161)

(5.162)

(5.163)

Let us now use some results from the analysis we performed a little while ago, with the integral method. Using the cubic velocity profile from this analysis, we have

 

 

u

=

3 y

1

y 2

 

 

 

 

 

 

 

 

 

 

 

 

 

u

2 δ

 

 

 

 

 

 

2

 

δ

 

u

=

3u

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

2δ

 

 

 

 

 

 

y y=0

 

 

 

 

 

 

Similarly the temperature profile turned out to be

 

 

 

 

(T T

)

 

 

3 y

 

1

 

y 3

 

 

θ =

 

 

 

= 1

 

 

 

+

 

 

 

 

 

 

 

(Tw T)

2 δT

 

 

 

 

 

 

 

 

 

2

 

δT

 

T

=

 

3

(Tw

T)

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

2δT

 

 

 

 

 

 

 

 

 

 

y y=0

 

 

 

 

 

 

 

 

 

 

 

 

 

Q

hA(Tw

T)

 

k × 2 × 3 × δ × (Tw T)

 

 

=

 

 

 

 

 

 

 

=

 

 

 

τ w A

 

 

×

1

Aρu2

 

 

2 × δT × µ × u× 3

 

c

 

 

 

 

 

 

 

f

 

2

 

 

 

 

 

 

 

h (Tw T)

=

 

k ×δ × (Tw T)

 

 

 

 

 

 

cf

×

1

 

2

 

 

δT × µ × u

 

 

 

 

 

 

2

ρu

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

(5.164)

(5.165)

(5.166)

(5.167)

(5.168)

(5.169)

Pr

(5.170)

 

 

 

k = cp

 

5.5 Turbulent flow 149

 

h × Pr

δT

 

=

cf

 

 

 

 

 

ρucp

 

 

 

δ

 

 

2

We know that δT /δ Pr1/3. Substituting for δT /δ in Eq. (5.171)

h × Pr × Pr-1/3

ρucp

c2f

The term within the brackets

c2f

=c2f

h

ρucp

 

h

 

 

 

 

 

 

ρu c

 

 

 

p

= St.Pr2 /3

Pr2 /3

is known as the Stanton number.

(5.171)

(5.172)

(5.173)

(5.174)

The above is known as the modified Reynolds analogy or the Chilton-Colburn

analogy, with the “plain” Reynolds analogy being

c f

= St for Pr = 1

fluids.

 

 

h

 

 

 

 

 

 

 

 

 

 

 

 

2

 

 

The term

 

can be simplified as follows.

 

 

ρc u

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

p ∞

 

 

h

 

 

 

Nu.k

 

 

 

 

 

 

 

 

 

 

=

 

 

 

 

 

(5.175)

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

ρcpu

L.ρucp

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

We know that

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

k

 

= α

 

 

 

 

(5.176)

 

 

 

 

 

ρcp

 

 

 

 

 

 

 

 

 

 

h

=

Nu α ϑ

=

Nu

= St

(5.177)

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

ρucp

 

uϑ L

ReL Pr

 

 

 

 

 

 

 

 

 

 

from Eq. (5.173),

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

c f

= St.Pr2 /3

 

(5.178)

 

 

 

 

 

 

 

 

2

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

In sum, once we have the skin friction coefficient, c f , using the modified Reynolds analogy, we can determine the Stanton number. From the Stanton number, we can estimate the Nusselt number and hence the heat transfer coefficient and finally the heat flux, q. Getting q or h is the fundamental challenge in convective heat transfer, as we have already emphasized.

The modified Reynolds analogy is valid for 0.6 < Pr < 60.

The analogy works very well for laminar flows with dp/dx = 0, but in turbulent flows, the sensitivity of heat transfer results to dp/dx is not significant, and the analogy holds. The analogy can be applied locally and also for the average coefficients over a geometry.

150 CHAPTER 5  Forced convection

From boundary layer measurements, for turbulent flow over a flat plate, the following critical information is available.

δ0.37

x= Rex0.2

and c

 

=

0.0592

, 5 ×105

Re

108

f ,x

Re0.2

 

 

 

x

 

 

 

 

x

 

 

 

With the above expression, using the modified Reynolds analogy, the local Nusselt number can be determined to be

Nux = 0.0296 Rex0.8 Pr0.33

(5.179)

Again, this is valid for fluids that satisfy 0.6 ≤ Pr ≤ 60

If the flow is mixed, that is, laminar up to x = xcrit and turbulent beyond, the average heat transfer coefficient hL is given by

 

=

1

 

xcrit hlaminar dx + L

hturb dx

(5.180)

hL

 

 

 

 

L

0

xcrit

 

 

Example 5.4: Consider a heated horizontal plate that is maintained at 100 °C. Air at 30 °C flows over with a velocity of 10 m/s. The plate area is 0.3 m2, and measurements reveal a drag force of 0.32 N on the plate by the flowing air. Determine the power (in W) that is required to maintain the plate at 100 °C.

Solution:

We use the modified Reynolds analogy to solve the problem. Air properties at 65 °C

ρ = 1.04 kg/m3 , ν = 19.51 × 106 m2 /s, k = 0.029 w/mK, Pr = 0.707, cp = 1.009 kJ/kgK

 

τ = c

 

.

1 ρu2

 

 

 

 

 

f

 

2

 

 

 

Drag force = τ × As

 

 

 

cf

=

Drag force

 

 

 

 

 

A

. 1

ρu2

 

 

 

 

 

 

s

2

 

 

 

 

cf

=

 

 

 

 

 

 

0.32

= 0.0205

 

0.3

×

1

×1.04 ×102

 

 

 

 

 

 

 

 

 

 

 

2

 

 

 

 

cf

=

 

 

h

 

 

 

 

 

2

ρucp

 

 

 

 

 

 

 

h =

0.0205

× 1.04 × 10 × 1009

 

 

 

 

 

2

 

 

 

 

 

h =107.6 W/m2K

Q = hA(τ w τ)

Q = 107.6 × 0.3(70) = 2260 W

5.6 Internal flows 151

Please note that the use of the modified Reynolds number analogy is an absolutely clever way to solve the problem. In fact, the length scale in the problem is not given and so ReL and NuL cannot be defined, but then these hardly mattered. We used the original definition of Stanton number, St = h/ρucp, to crack the problem. Additionally, from the friction data, we got the heat transfer. This is vintage engineering heat transfer.

5.6  Internal flows

Forced convection inside tubes and ducts has a very large number of applications, starting from the pipe carrying hot steam from the boiler to the turbine in a thermal power plant, to the tubes carrying the refrigerant in the condenser and evaporator of a refrigerator, and the tubes carrying the coolant in any automobile radiator or in any heat exchanger, for that matter.

The key challenge in the above mentioned applications is the calculation of the heat transfer coefficient h for the internal flow inside the tube in a particular application. Stated explicitly, if a constant heat flux or constant wall temperature on the outside of a tube (due to, say, vapor condensing on the outside), the key challenge is to get "h" for the fluid flowing inside the tube. In the more general case, along with this, the heat transfer coefficient on the outside, the conduction resistance across the tube material and any fouling resistance all have to be considered to obtain the overall heat transfer coefficient, which was briefly introduced in Chapter 1.

The key difference between external flows and internal flows is the concept of “developing” and “fully developed” flow, which can be best understood from a figure.

Consider a circular tube of diameter, d. A fluid enters the tube at x = 0 (see Fig. 5.8). Once the fluid enters the duct all over the surface, the presence of wall will be felt by the viscous fluid. Hence, a boundary layer starts developing as indicated in the figure. Once the boundary layer thickness δ becomes d /2, the whole of the flow inside the tube becomes a boundary layer flow, as opposed to the flat plate, where beyond y = δ in the free stream, the effects of fluid viscosity are not felt. The length X at which the whole of the flow becomes a full boundary layer flow is called entry length, and the flow beyond X, is known as “fully developed.”

FIGURE 5.8

Concept of developing flow inside a tube.

152 CHAPTER 5  Forced convection

We can work out the ballpark estimates of this entry length from the boundary layer results applicable for external flow.

We earlier estimated the boundary layer thickness for forced convection over a flat plate to be

 

δ

 

5

 

x

 

Rex

 

 

 

or, δ ≈ 5

ν x

 

 

 

 

u

 

 

 

 

δ = d /2 when x X, where X is the entry length.

 

 

 

d

= 5

ν X

 

2

u

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

d2

 

 

= 25

ν X

 

4

 

 

u

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

X

1

 

 

ud

 

 

 

 

 

 

=

 

 

 

 

 

 

 

 

 

d

 

 

100

 

ν

 

 

X

≈ 102

ud

≈ 10

2 Re

 

 

 

 

d

 

 

 

 

 

 

 

ν

d

 

 

 

 

 

 

 

 

 

 

(5.181)

(5.182)

(5.183)

(5.184)

(5.185)

A more exact estimate of X/d that is frequently used in literature is 0.05Red For turbulent flow X /d is approximately 10 and is indeed very short. The idea of fully developed flow can be exploited to our advantage, if we want to get a handle on the analytical treatment of fluid flow and heat transfer in tubes and ducts, as it is intuitively apparent that the governing equation should simplify in the fully developed region. Even so, discerning readers will quickly realize that since the boundary layer thickness is smaller in the developing region of the flow, the local heat transfer coefficient, in whichever way we want to define, will be high. Hence, many short tubes instead of a few longer tubes may do the trick sometimes. Even so, there may be other considerations such as pressure drop, the sheer arrangement of tubes, and so on. So, a decision to work with shorter or longer tubes eventually is an engineering compromise.

5.6.1  Governing equations and the quest for an analytical solution

Consider two-dimensional, steady, laminar, incompressible flow with constant properties inside a pipe. The governing equations derived in Cartesian coordinates will look like what are shown below in the cylindrical coordinates.

Continuity equation

u

+

1 (vr)

= 0

(5.186)

 

 

 

x

r r

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

5.6 Internal flows 153

Momentum equations

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

x momentum

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

ρ

 

u

+ v

u

= −

p

 

 

2 u

+

1

u

+

2 u

 

 

(5.187)

 

 

u

x

 

 

x

+ µ

x2

r

r

r2

 

 

 

 

 

 

 

 

 

r

 

 

 

 

 

 

 

 

 

 

 

 

r momentum

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

v

 

v

 

 

p

 

 

2 v

1 v

 

v

 

2 v

 

 

ρ u

 

 

 

+ v

 

= −

 

 

+

µ

 

 

 

+

 

 

 

 

 

 

+

 

 

 

(5.188)

 

x

r

 

x

2

r r

 

r

2

r

2

 

 

 

 

r

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

The geometry, coordinate axes, and the respective velocities are given in Fig. 5.9.

Comparing the scales of the two terms in the continuity equation, we have

 

v

 

U

 

(5.189)

 

D

 

x

 

 

 

v

UD

(5.190)

x

 

 

 

 

 

Therefore, as x increases, v decreases. So, as we proceed deeper (i.e., into the fully developed region), v = 0.

From the continuity equation, in the fully developed flow region, ux = 0.

u = f (r) alone

(5.191)

Substituting for v = 0 in the r momentum equation, with the understanding that v and all its derivatives are zero in the fully developed region, the r momentum equation reduces to p/ r = 0. Hence p/ x in Eq. (5.187) can be simplified as dp/dx . Eq. (5.187) now becomes

d 2u

 

1 du

 

dp

 

 

 

 

+

 

 

 

=

 

(5.192)

 

2

 

dx

dr

 

 

r dr

 

 

FIGURE 5.9

Problem geometry, coordinates, and velocities for laminar flow inside a pipe.

154 CHAPTER 5  Forced convection

Please note that Eq. (5.192) is an ordinary differential equation, while Eq. (5.187) is a partial differential equation. The above equation can be solved with the following two boundary conditions.

 

 

 

 

At

r = r0

or d / 2, u = 0 (no slip)

 

 

 

 

At

r = 0,

 

du

= 0

(symmetry)

 

 

 

 

 

 

dr

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

1 d

 

du

=

dp

 

 

 

 

 

 

 

r

 

 

 

 

 

 

 

 

 

 

 

 

 

 

dx

 

 

 

 

r dr

 

dr

 

 

 

 

 

Integrating twice

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

u =

1

dp r2

+ Alnr + B

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

dx 4

 

(5.193)

(5.194)

(5.195)

(5.196)

From the boundary conditions, at r = r0 , u = 0 and at r =0, du / dr = 0,

A = 0 and B = −

1

dp r2

 

 

 

 

 

0

.

 

 

4

 

dx

 

 

r2

 

dp

 

 

r 2

u = −

0

 

1

 

 

 

 

 

 

 

 

 

 

 

4 dx

 

 

r

 

 

 

 

 

 

 

0

 

 

 

 

 

 

 

 

 

 

 

we have

(5.197)

Hence, the velocity profile for fully developed laminar flow in a pipe is parabolic. The above is also referred to as the Hagen-Poiseulle flow. As we already saw,

p = f (x) alone; the x momentum equation can be rewritten as

dp

d2u

 

1 du

 

 

 

=

 

 

+

 

 

 

= C

(5.198)

dx

 

2

 

dr

 

 

r dr

 

 

Since the left-hand side of the above equation is a function of x and the righthand side of the equation is a function of r alone, both have to be equal to a constant C.

If the entry length xis much smaller than L, where L is the length of the tube under consideration, the relation dp/dx = C can be extended to the “small” entry length too (with an added error, though) so that

dp

 

p

(5.199)

dx = −

L

 

Please note that the struggle in fluid mechanics is to get the pressure drop, p. . The average or mean velocity can now be calculated using the mass flow rate m

m

= r0

ρ u(r) 2π r dr = ρum π r02

(5.200)

 

0

 

 

 

 

 

 

 

 

 

2

 

r0

r2

dp

r 2

 

um

=

 

 

 

0

 

1−

 

.rdr

(5.201)

2

 

 

4

 

 

 

 

r0

 

0

dx

r0

 

u

=

1

dp r2

r4 r0

=

−r2

dp

 

 

 

 

 

0

 

m

 

 

 

 

 

 

 

 

 

 

 

 

 

2

dx

2

4r02

 

8 dx

 

 

 

 

 

 

 

 

0

 

 

 

The maximum velocity umax occurs at r = r0 .

umax = r02 dp 4 dx

5.6 Internal flows 155

(5.202)

(5.203)

comparing Eqs. 5.202 and 5.203, we have umax = 2um . Now we proceed to evaluate the shear stress, , and the skin friction coefficient, c f .

 

τ = µ

 

∂u

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

∂r

r =r0

 

 

 

 

τ = µ

−r

2

 

 

 

r

 

 

 

 

 

 

 

 

 

 

0

 

 

 

 

 

 

 

 

 

4µ

r02

 

r =r0

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

τ =

r0

 

dp

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

2 dx

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

However, from the expression for um we have

 

 

 

 

dp

 

 

8 um

 

 

 

 

 

 

 

 

 

 

 

= −

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

dx

 

 

 

 

r2

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

0

 

 

 

 

 

 

 

 

 

 

 

 

 

τ =

r0

 

 

8

 

um

 

 

 

2

 

 

 

 

 

r

2

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

0

 

 

 

 

 

 

 

τ =

 

 

4 um

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

r

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

0

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

4 um

 

 

cf =

 

 

 

 

τ

 

 

=

 

 

 

 

r0

 

 

 

1

ρum2

 

1

 

ρum2

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

2

 

 

 

 

 

 

 

 

 

 

 

2

 

 

 

 

This is also known as the Fanning friction factor,

16

 

16

=

 

=

 

um D

Re

 

 

 

D

 

ν

 

 

 

 

f .

f = cf = 16

ReD

The Darcy-Weisbach friction factor, fD, is given by

fD = 4 f = 64

ReD

(5.204)

(5.205)

(5.206)

(5.207)

(5.208)

(5.209)

(5.210)

(5.211)

(5.212)

For turbulent flows, measurements confirm the following expressions for friction factors.